Soil Water Dynamics In Burned Areas After A Late Summer Rain. The Role Of Fire Intensity, Microsite, Sampling Depth, And Time Of Measurement
Price
Free (open access)
Transaction
Volume
22
Pages
10
Published
1997
Size
980 kb
Paper DOI
10.2495/ECOSUD970551
Copyright
WIT Press
Author(s)
M.J. Molina & J.V. Llinares
Abstract
In Mediterranean areas, where fire is a recurrent process, soil water availability may be a major cause for the spatial and temporal pattern of plant recovery after fires, since water is found to limit plant growth in semiarid environments. In the Spanish region of Valencia we studied the water dynamics of a typical forest soil subjected to experimental fires of contrasted levels of fire intensity, and also that of a control (unburned) soil. This was done in the field by TDK examination of their water content variations at the 0-10 mm surface soil and at the 10-100 mm subsoil, in the plant spaces and the plant interspace patches, after the first intense rainfall followi
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